摘要
Observations from regional seismic network are used in studying deviatoric moment tensor for the MW5.4 earthquake of 26 Febuary 2010 in Taiwan adjacent area.The smallest rotation angle defined by Kagan (1991) between the result and the Havard GCMT solution is 9.5°, and the focal depth is 41 km, which is close to USGS location result and possibly closer to the real source.The paper also discusses the effect of station distribution on deviatoric moment tensor inversion by selecting different station combinations.